Low-sulfide PGE-Cu-Ni Mineralization from Five Prospects within the Footwall of the Sudbury Igneous Complex, Ontario, Canada
North Range low-sulfide mineralization is dominantly hosted by Sudbury breccia, with amphibole-plagioclase equilibrium metamorphic temperatures of 440 to 533 ± 75oC, produced by the SICs thermal aureole. Mineralization led to increases in the bulk halogen content of the host Sudbury breccia and the...
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| Language: | en_ca |
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2012
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| Online Access: | http://hdl.handle.net/1807/32849 |